Hydrologic Response to Future Climate Change in the Dulong-Irra-waddy River Basin Based on Coupled Model Intercomparison Project 6

Within the context of the Belt and Road Initiative(BRI)and the China-Myanmar Economic Corridor(CMEC),the Dulong-Ir-rawaddy(Ayeyarwady)River,an international river among China,India and Myanmar,plays a significant role as both a valuable hydro-power resource and an essential ecological passageway.However,the water resources and security exhibit a high degree of vulnerabil-ity to climate change impacts.This research evaluates climate impacts on the hydrology of the Dulong-Irrawaddy River Basin(DIRB)by using a physical-based hydrologic model.We crafted future climate scenarios using the three latest global climate models(GCMs)from Coupled Model Intercomparison Project 6(CMIP6)under two shared socioeconomic pathways(SSP2-4.5 and SSP5-8.5)for the near(2025-2049),mid(2050-2074),and far future(2075-2099).The regional model using MIKE SHE based on historical hydrologic processes was developed to further project future streamflow,demonstrating reliable performance in streamflow simulations with a val-idation Nash-Sutcliffe Efficiency(NSE)of 0.72.Results showed that climate change projections showed increases in the annual precip-itation and potential evapotranspiration(PET),with precipitation increasing by 11.3%and 26.1%,and PET increasing by 3.2%and 4.9%,respectively,by the end of the century under SSP2-4.5 and SSP5-8.5.These changes are projected to result in increased annual streamflow at all stations,notably at the basin’s outlet(Pyay station)compared to the baseline period(with an increase of 16.1%and 37.0%at the end of the 21st century under SSP2-4.5 and SSP5-8.5,respectively).Seasonal analysis for Pyay station forecasts an in-crease in dry-season streamflow by 31.3%-48.9%and 22.5%-76.3%under SSP2-4.5 and SSP5-8.5,respectively,and an increase in wet-season streamflow by 5.8%-12.6%and 2.8%-33.3%,respectively.Moreover,the magnitude and frequency of flood events are pre-dicted to escalate,potentially impacting hydropower production and food security significantly.This research outlines the hydrological response to future climate change during the 21st century and offers a scientific basis for the water resource management strategies by decision-makers.

Comparative Study of the Physicochemical Quality of the Waters of the Méné River (Sassandra Watershed, Ivory Coast) in the Dry Season and in the Rainy Season

The study carried out on the waters of the Méné River led to an overall assessment of its water quality during the dry season and the rainy season. The analysis focused on eight (8) water samples taken from the river during a period of dry season (January-February) and a period of rainy season (June and September). The various physicochemical parameters were measured according to Afnor standardized methods. The readings of temperature, turbidity, pH and conductivity made it possible to account for the disturbances occurring in water quality. A temporal variation correlated with the seasons (dry or rainy) is noted. Turbidity depends on the concentration of suspended solids (SS) in the water and drained particles and therefore on the seasons. Just like the temperature, the conductivity changes with the season. The waters of the Méné River are generally acidic. The results obtained show that there is a low level of pollution by chlorides, phosphates, nitrites and nitrates. A slight pollution of the waters of Méné in organic matter (chemical oxygen demand values are less than 25 mg∙L−1 during dry season and 32.33 ± 4.73 mg∙L−1 during rainy season) was observed. The concentrations of metallic trace elements such as iron, manganese and aluminum indicate significant pollution of these waters by these elements. Overall, the waters of the Méné River are of satisfactory quality because all the physicochemical parameters analyzed have values below standards during the dry season as well as during the rainy season with the exception of COD and a few metallic trace elements.

基于N-CMIP6的长江流域气温和降水未来预估

为探究具有更高可信度的长江流域未来气温和降水的时空变化特征,基于1961~2020年中国格点化逐日气象观测数据,采用2022年最新发布的NASA高分辨率降尺度数据集(N-CMIP6)中的35个气候模式对长江流域气温和降水模拟能力进行了评估,进而预估了不同共享社会经济路径(SSPs)情景下(SSP1-2.6、SSP2-4.5、SSP3-7.0和SSP5-8.5)长江流域在21世纪近期(2021~2040年)、中期(2041~2060年)和末期(2081~2100年)气温和降水的时空演变特征。结果表明:2021~2100年,长江流域年均气温和降水均呈现显著上升趋势,尤其是上游地区增温最为明显;到21世纪末期(2081~2100年),相较于基准期(1995~2014年),长江流域平均气温预计将升高1.61~5.18℃,平均降水量将增加7.6%~12.8%;秋季温度升高最为显著,其次是夏季,冬季降水增幅最大,秋季次之。研究成果有助于深化对区域气候变化的科学理解,为政府决策提供科学依据,以有效应对和适应气候变化带来的挑战,进而促进可持续发展。

基于Landsat8的沱沱河流域总氮和氨氮反演模型研究

将沱沱河流域2021年6-7月TN、NH_(3)-N的实测值和Landsat 8影像的41种波段组合的反射率建立反演关系,筛选出拟合度较高的波段组合与实测值以线性、二次多项式、对数函数、指数函数和幂函数的方式建立反演模型。结果表明,Landsat 8影像的B4、B5、B6和B7波段反射率与TN、NH_(3)-N值呈显著相关性;B4+B5+B7波段组合与TN值具有较高的拟合度,B6/B7与NH3-N值具有较高的拟合度。将2021年8月的遥感影像利用模型反演TN、NH_(3)-N的预测值,并与实测值进行模型精度验证,TN值反演模型的MAE为13.89%,RMSE为0.152 mg/L,NH_(3)-N值反演模型的MAE为5.87%,RMSE为0.077 mg/L。

Prospects for Minimizing the Potential Environmental Impacts of the Hydro-Agricultural Dam of M’Bahiakro(Cote d’Ivoire)

This study aims at characterizing the physical environment and suggesting solutions for a better management of the hydro-agricultural dam of M’Bahiakro which is being constructed over the N’Zi River and is the first inflatable dam in Cote d’Ivoire. In this survey, data related to hydrology, characteristics of the dam and the irrigated rice production area were obtained with the Water Resources Agency and the National Office of Rice Development of Cote d’Ivoire. Physicochemical parameters of the N’Zi River were collected seasonally at three monitoring stations. Results showed that the N’Zi River is characterized by a high water level period from April to November and a low water level period from November to April. The gap between the low flows and the high flows is important (about 206 m3/s on average). The annual average flow is 40 m3/s with a standard deviation of 32.52 m3/s and a variation coefficient of 0.88. The SAR average value (1.63) and the average conductivity (78.44 μS/cm) showed that waters of the N’Zi River are of high quality to be used for irrigation. Suspended sediment concentrations do not present significant difference along the river. But the seasonal variations are important;they are higher during the rainy seasons (45.8 mg/L on average) than in the dry seasons (17.7 mg/L on average). The annual solid flux of the N’Zi River is 41897 tons, i.e. 15810 m3 of sediments. The annual sediment flux is important and can lead to high depositions in the line-shaped reservoir of the dam and that calls for attention to control the silting up of the reservoir. Great efforts concerning interdisciplinary approaches, as well as extensive and intensive field work are needed in order to better manage the hydro-agricultural dam of M’Bahiakro.

长江流域30°N沿线昼夜及冬夏降水特征差异分析

利用1996—2020年逐时降水资料,统计分析长江流域30°N沿线不同地形阶梯代表区昼、夜、冬、夏降水的频率、雨量、类条件概率密度等特征,通过研究昼夜比、冬夏比随经度的分布探讨不同高度地形对降水的影响。主要结论如下:(1)30°N沿线四川盆地内降水量和频率的夜昼比向东递减,雅安附近是夜雨强中心区,夜雨现象在四川盆地东侧山地108°E以东趋于消失;盆地内强降水比弱降水更易发生于夜间。(2)30°N沿线冬雨与夏雨存在较大差异,雨量上冬雨小、夏雨大;结构上冬雨弱、夏雨强;降水频次上存在地域差异,第二地形阶梯冬雨少、夏雨多,而第三地形阶梯反之;冬雨受大地形影响更为明显。(3)根据降水第1类类条件概率密度(CCPD1)冬夏比及冬雨CCPD1距平百分比聚类分析,可将8个分区分为3类,该分类与地理位置、地形阶梯有良好的对应关系。(4)夏雨受局地地形影响显著,将夏雨CCPD1距平百分比高于10%的峰(低于-10%的谷)值区定义为夏雨强(弱)潜力区,则各分区强、弱潜力区表现各异。江汉平原南部、鄱阳湖以北发生短时强降水潜力较大,雅安出现极端短时强降水潜力大(强潜力区≥61 mm);冬雨强潜力区(CCPD1距平百分比高于50%的峰值区)位于第三地形阶梯上的Ⅶ、Ⅷ、Ⅸ分区(潜力值1~20 mm),而该降水区间也是雅安和盆地中央的弱潜力区(CCPD1距平百分比低于-50%的谷值区)。

Characteristics of nutrients in the Jiulong River and its impact on Xiamen Water, China

Water samples were collected at 20 sites on 4 occasions in 2009 （twice in May, and once in both August and November） along the Jiulong River, South China to examine how nutrient inputs from the Jiulong River could affect the nutrient status of the Xiamen Water. Samples were analyzed for nitrite （NO2-N）, nitrate （NO3-N）, ammonium （NH4-N）, phosphate （PO4-P）, silicate （SiO3-Si）, salinity, and temperature, to determine the nutrient and trophic status of the river. The results indicate that nutrients are derived mainly from river runoff. NO3-N was the main form of DIN in most parts of the river. In addition, NO3-N, DIN, and SiO3-Si behave conservatively. There is a surplus of DIN and SiO3-Si in the river, and PO4-P is a limitation on phytoplankton growth. The concentration of DIN is typically above 0.60 mg/dm3, and higher than 1.00 mg/dm3 in most parts of the river. The concentration of PO4-P is typically above 0.02 mg/dm3, while the concentration of SiO3-Si is higher than 1.00 rag/din3. Between 2003 and 2008, samples were collected 3 times per year （May, August and November） at 27 sites in the Xiamen Water and analyzed for NO2-N, NO3-N, NH4-N, PO4-P, salinity, and temperature. We discovered that the Jiulong River was the key source of DIN into the Xiamen Water, but not PO4-P, indicating the reason of the N/P molar ratio imbalance in the Xiamen Water. In the future, the effects of high DIN concentrations on the phytoplankton communities and marine ecosystems of the Xiamen Water shall be studied.

Assessment of bacterial biomass in the highly contaminated urban Nanming River,Guiyang,SW China

High anthropogenic N loads and abundant bacteria are characteristic of highly contaminated urban rivers.To better understand the dispersal and accumulation of bacteria, we determined contents and isotopic compositions of suspended particulate organic matter(SPOM) and bacteria in a highly contaminated urban river(the Nanming)and effluents in winter and summer of 2013. Relative to SPOM, bacterial biomass in the river was depleted in ^(13)C and ^(15)N and its C/N ratio was lower(δ^(13)C:-33.2% ± 3.1%; δ^(15)N:-1.5% ± 1.2%; C/N:4.8 ± 0.6), while effluents showed higher ^(13)C and ^(15)N contents and C/N ratios(δ^(13)C:-25% ± 2.1%; δ ^(15)N:-8.5% ± 1.1%; C/N: 8.1 ± 1.2). Source recognition of SPOM was based on carbon isotopes because they are conservative and distinct between end-members(effluent detritus and bacterial biomass). Using a mixing model,bacterial biomass in the river was calculated to account for <20% and <56% of bulk suspended particulate organic nitrogen in winter and summer, respectively. An N budget showed that bacterial N was a small proportion of total nitrogen(<7.4%) in the riverwater.

甘南黄河流域4种典型林分土壤C、N、P化学计量特征

土壤碳(C)、氮(N)、磷(P)是参与植物光合作用和影响生态系统初级生产力的主要元素。甘南高原是黄河流域重要的生态屏障,为了解该区不同林分土壤养分状况的差异,选取该区4种典型林分:云杉林、华北落叶松林、巴山冷杉林以及岷江冷杉糙皮桦混交林为研究对象,研究土壤C、N、P化学计量特征。结果表明:(1)岷江冷杉及糙皮桦混交林土壤C、N含量最高,云杉林土壤N、P含量最低。不同林分间P含量差异显著(P<0.05),不同土层间C、N含量差异均显著(P<0.05)。(2)云杉林土壤C∶N值显著高于其他林分,岷江冷杉及糙皮桦混交林土壤N∶P及C∶P高于其他林分。(3)海拔、土壤pH、容重与土壤含水量是影响土壤养分的重要因素。土壤C含量与N、P含量均显著相关(P<0.05)。总体来说,不同林分土壤化学计量特征具有显著差异,混交林土壤养分状况较纯林好,未来森林管理和植被建设中,可以通过选择合适的树种和提高树种多样性有效改善森林土壤质量。

Composting Efficiency of Urban Forest Litter and River Sediment at Different Proportions

In order to explore a technology for producing organic fertilizer by composting urban forest litter and river sediment passivated by fly ash, an experiment was conducted to study dynamic changes of several parameters including temperature, pH, organic matter, C/N and germination index （GI） during high-temperature composting of urban forest litter and river sediment at five different proportions （1：1 （Ⅰ）, 1：2 （Ⅱ）, 1：3 （Ⅲ）, 2：1 （Ⅳ） and 3：1 （Ⅴ））. Results showed that the temperature and pH increased first and then decreased; at the proportion of 3：1, the temperature increased rapidly and the high-temperature duration was longest （5 d）; at the end of the composting, all the treatments reached the decomposed status, the pH ranged from 7.47 to 8.87, and the organic matter content was reduced by 36%, 38%, 42%, 33% and 29%, respectively, indicating that increasing the proportion of urban forest litter was conducive to reducing the loss of organic matter. Due to low C/N ratio of river sediment, increasing the proportion of urban forest litter was helpful to improve the efficiency of composting. The GI of treatments I, IV and V reached 80% on day 26, 18 and 19 respectively, but the GI of treatments II and III did not reach this level until the end of composting. Considering the quality of fertilizer and efficiency of composting for large-scale production, the proportion between urban forest litter and river sediment is suitable to be set as 3：1 for production of organic fertilizer.

Spatial Variability of Soil Carbon to Nitrogen Ratio and Its Driving Factors in Ili River Valley,Xinjiang,Northwest China

Soil carbon to nitrogen(C/N) ratio is one of the most important variables reflecting soil quality and ecological function,and an indicator for assessing carbon and nitrogen nutrition balance of soils.Its variation reflects the carbon and nitrogen cycling of soils.In order to explore the spatial variability of soil C/N ratio and its controlling factors of the Ili River valley in Xinjiang Uygur Autonomous Region,Northwest China,the traditional statistical methods,including correlation analysis,geostatistic alanalys and multiple regression analysis were used.The statistical results showed that the soil C/N ratio varied from 7.00 to 23.11,with a mean value of 10.92,and the coefficient of variation was 31.3%.Correlation analysis showed that longitude,altitude,precipitation,soil water,organic carbon,and total nitrogen were positively correlated with the soil C/N ratio(P < 0.01),whereas negative correlations were found between the soil C/N ratio and latitude,temperature,soil bulk density and soil p H.Ordinary Cokriging interpolation showed that r and ME were 0.73 and 0.57,respectively,indicating that the prediction accuracy was high.The spatial autocorrelation of the soil C/N ratio was 6.4 km,and the nugget effect of the soil C/N ratio was 10% with a patchy distribution,in which the area with high value(12.00–20.41) accounted for 22.6% of the total area.Land uses changed the soil C/N ratio with the order of cultivated land > grass land > forest land > garden.Multiple regression analysis showed that geographical and climatic factors,and soil physical and chemical properties could independently explain 26.8%and 55.4% of the spatial features of soil C/N ratio,while human activities could independently explain 5.4% of the spatial features only.The spatial distribution of soil C/N ratio in the study has important reference value for managing soil carbon and nitrogen,and for improving ecological function to similar regions.

Particulate n-alkanes and fatty acids in the Changjiang river system

Particulate samples were collected from the Changjiang river system during a flood period, in May 1997, and POC, stable isotope and lipids associated with particles were examined. Results showed the decrease （0.84% ～ 1.88%） of organic carbon content from the upper reaches to the estuary.δ^13 values of particulate organic carbon was in the range of -24.9×10^-3 to -26.6×10^-3, which were close to the isotopic signature of continental C3 vegetation. Total particulate n-alkanes concentrations varied from 1.4 to 10.1μg/dm^3,or from 23.7 to 107μg/g of total suspended matter. Fatty acids were present in all the samples, from 1.4 to 5.4μg/dm^3, with saturated and unsaturated straight-chain and branched compounds in the carbon number range from C12 to C30. Both δ^13 and the ratio of carbon content to nitrogen content indicate the predominance of terrestrial inputs （soil organic matter） among the particles. The biomarker approach has been used to identify the relative portion of terrigenous and autochthonous fraction in the particulate samples. The distribution of fatty acids suggests a striking phytoplanktonic and microbial signal in most particle samples. The terrestrial alkanes are used to estimate the contribution of terrestrial inputs along the mainstream.

The Signatures of Stable Isotopes δ^(15)N and δ^(13)C in Anadromous and Non-Anadromous Coilia nasus Living in the Yangtze River, and the Adjacent Sea Waters

Stable isotopes are increasingly used to investigate seasonal migrations of aquatic organisms. This study employed stable isotopes (delta C-13 and delta N-15) for Coilia nasus from the lower Yangtze River and the adjacent East China Sea to distinguish different ecotypic groups, ascertain trophic nutrition positions, and reflect environmental influences on C. nasus. delta C-13 signatures of C. nasus sampled from Zhoushan (ZS), Chongming (CM), and Jingjiang (JJ) waters were significantly higher than those from the Poyang Lake (PYL) (P < 0.05). By contrast, delta N-15 signatures of C. nasus in ZS, CM, and JJ groups were significantly lower than those in PYL group (P < 0.05). Basing on delta C-13 and delta N-15 signatures, we could distinguish anadromous (ZS, CM, and JJ) and non-anadromous (PYL) groups. The trophic level (TL) of anadromous C. nasus ranged from 2.90 to 3.04, whereas that of non-anadromous C. nasus was 4.38. C. nasus occupied the middle and top nutrition positions in the marine and Poyang Lake food webs, respectively. C. nasus in Poyang Lake were significantly more enriched in delta N-15 but depleted in delta C-13, suggesting that anthropogenic nutrient inputs and terrigenous organic carbon are important to the Poyang Lake food web. This study is the first to apply delta N-15 and delta C-13 to population assignment studies of C. nasus in the Yangtze River and its affiliated waters. Analysis of stable isotopes (delta N-15 and delta C-13) is shown to be a useful tool for discriminating anadromous and non-anadromous C. nasus.

Stable Carbon Isotope and Long-Chain Alkane Compositions of the Major Plants and Sediment Organic Matter in the Yellow River Estuarine Wetlands

Elemental(TOC,TN,C/N)and stable carbon isotopic(δ^13C)compositions and long-chain alkane(n C16-38)concentrations were measured for eight major plants and a sediment core collected from the Yellow River estuarine wetlands.Our results indicate that both C3(-25.4‰to-29.6‰)and C4(-14.2‰to-15.0‰)plants are growing in the wetlands and C3 plants are the predominant species.The biomass of the wetland plants had similar organic carbon(35.5-45.8%)but very different organic nitrogen(0.35-4.15%)contents.Both C3 and C4 plants all contained long-chain alkanes with strong odd-to-even carbon numbered chain predominance.Phragmites australis,a dominant C3 plant contained mainly n C29 and n C31 homologues.Aeluropus littoralis,an abundant C4 plant were concentrated with n C27 and n C29 homologues.Organic matter preserved in the Yellow River estuarine sediments showed strong terrestrial signals(C/N=11-16,δ^13C=-22.0‰to-24.3‰).The distribution of long-chain n-alkanes in sediments also showed strong odd-to-even carbon chain predominance with n C29 and n C31 being the most abundant homologues.These results suggest that organic matter preserved in the Yellow River estuarine sediments were influenced by the wetland-derived organic matter,mainly C3 plants.The Yellow River estuarine wetland plants could play important role affecting both the carbon and nutrient cycling in the estuary and adjacent coastal waters.

Generation and transmission of greenhouse gases in river system

The research progress on the current domestic and foreign about river water system of the greenhouse gas methane(CH4),and nitrous oxide(N2O)generation,transmission and release mechanism are reviewed in this paper.At present,at home and abroad of river water system of methane production and release of the driving factors and mechanism has been basically clear,but the N2O production mechanism is not clear,multi factor interaction of river water system of N2O production and release of complex,in different regions and time of result differences.The calculation of water flux of N2O river discharge coefficient of river IPCC released based on N2O,the release amount may underestimate the river water N2O.

Ion Selective Electrode Determination of Ammonia Nitrogen in Passaic River Waste Water in New Jersey Essex County Area

The percent ammonia nitrogen was determined in Passaic River waste water using Ion-Selective Electrode EPA Method 350.3. The intelligent ammonia sensor integrates ammonia electrode, pH electrode and Ammonia Ion electrode together to realize the in situ detection of ammonia. The test results have shown that the sensor is easy operation, low cost and no pollution. The ammonia is determined potentiometrically using an ammonia ion selective electrode and a pH/mV meter, having an expanded millivolt scale. The ammonia selective electrode uses a hydrophobic gas-permeable membrane to separate the sample solution from an electrode internal solution of ammonium chloride. Dissolved ammonia is converted to NH3 gas by raising the pH to above 11.0 with a strong base. NH3 gas diffuses the membrane and changes the internal solution pH that is sensed by the electrode. In single laboratory test results have been found 1.001 NH3-/L and 0.897 mg NH3-N/L, recoveries were 77.3% and 83.1%, respectively.

岷江流域COD、NH_(3)-N通量与排放总量、环境容量、环境质量分析研究

水是维护人类生活和社会稳定的核心自然要素。近几十年来伴随我国改革开放带来的社会经济跨越式发展,水污染问题日益突出,水环境质量明显下降,严重地影响了人民的生产、生活及周边的生存环境。要解决水污染问题,首先应确定水环境容量,控制污染物排放总量。因此,文章基于四川省污染源调查、四川省年度环统数据分析和在线四川省环境监测数据,在岷江流域进行水质检测数据收集;对岷江流域区域污染物通量与排放总量、通量以及环境质量进行综合分析,采用功能区控制法分别计算了化学需氧量(Chemical Oxygen Demand,COD)、氨氮(Ammonia Nitrogen,NH3-N)水环境容量,以期对水环境发展变化做出更符合实际的结论和预测。

长江口柱状沉积物中有机质C/N比的研究

对长江口四个站位沉积物中有机质的C/N比在垂向上的分布进行了研究,在影响沉积物中有机质C/N比的环境因素中,上覆水体的水深、盐度、密度以及浊度对其有一定的影响.在研究沉积物中有机质C/N比的分布及其影响因素的基础上,进一步估算了陆源输入和海洋自生有机碳在这四个站位沉积物有机碳中所占的比例,结果表明,海洋自生组分占沉积物总有机碳的比例分别为:53.57%(8号站位)、20.34%(11号站位),12.28%(17号站位)和32.73%(26号站位).

内蒙古草甸草原CH_4和N_2O排放通量的时间变异

1998年 6月 1日、7月 2日、8月 3日和 9月 1日用静态箱_气相色谱法对内蒙古锡林河流域草甸草原CH4和N2 O排放通量的昼夜观测表明 ,天然草原是N2 O的源、CH4的汇 ,其排放和吸收具有明显的昼夜变化规律。 4次昼夜观测的结果还表明 ,草甸草原排放N2 O和吸收CH4的能力具有强烈的季节变化规律。方差分析表明 ,不同季节N2 O排放通量差异显著 (F =6 .35 9,p <0 .0 0 4 ) ,日均通量变化范围为 0 .2 82～ 2 .134μgN2 O N·m-2 ·h-1;而CH44次测定的日均吸收通量分别为 (- 5 2 .19± 19.6 7)、(- 2 7.2 0± 10 .5 7)、(- 12 6 .0 5± 9.32 )和 (- 16 .4 5± 1.31) μgCH4_C·m-2 ·h-1,从整个生长季看表现为“高_低_高_低”的特点。锡林河流域选择 9∶0 0～ 13∶0 0作为采样日起始采样时间 。

乌江重庆段水体的COD_(Mn)、氮和磷的时空分布

以2008年乌江水质的调查数据为依据,研究了乌江重庆段万木、鹿角、锣鹰段、武隆和麻柳嘴断面水体中的CODMn、氮、磷的空间分布特征.结果表明,乌江重庆段武隆断面TN质量浓度均值为2.317 mg/L,其中无机氮为2.107 mg/L,占TN的90.93%;NO-3-N为2.022 mg/L,占无机氮总量的95.97%,TN质量浓度呈现丰水期>枯水期>平水期.TP均值为0.173 mg/L,TP质量浓度呈现夏季>冬季>春秋季,丰水期>其他水期;总CODMn与颗粒态CODMn的变化规律一致,均表现为丰水期>平水期>枯水期;N、P、CODMn在水深方向变化不明显;NH+4-N的全年质量浓度均值按照万木、鹿角、锣鹰段、武隆依次降低,到麻柳嘴断面回升.CODMn在水流沿程方向总体呈现出上游断面质量浓度较高,随水流方向各断面质量浓度总体呈下降趋势,在麻柳嘴断面处回升.营养盐在麻柳嘴断面的质量浓度有所回升,可能是三峡水库蓄水导致江水回荡,使其质量浓度升高.